1983
DOI: 10.1364/ao.22.000190
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Simulation of IR images of natural backgrounds

Abstract: Two schemes for the simulation of IR images of ground terrain are presented. Both preserve the statistics and power spectra of the temperature variation over the scene according to the experimental findings. The first scheme generates the scene directly in the spatial domain, while the second generates it in the spatial-frequency domain. Each is advantageous according to the simulation task needed.

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Cited by 29 publications
(5 citation statements)
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“…There is a precondition that the non-parametric random field models are all based on the normal distribution. Simultaneously, the temperature field of the terrain can be regarded as a 2D normal Markov process [10] . We can convert the synthesized textures to temperature fields using a transformation by given the average temperature and the standard variation.…”
Section: Convert Texture To Temperature Fieldmentioning
confidence: 99%
“…There is a precondition that the non-parametric random field models are all based on the normal distribution. Simultaneously, the temperature field of the terrain can be regarded as a 2D normal Markov process [10] . We can convert the synthesized textures to temperature fields using a transformation by given the average temperature and the standard variation.…”
Section: Convert Texture To Temperature Fieldmentioning
confidence: 99%
“…There are a number of different approaches to choose from when generating the height-data for ocean surface 8 . The Navier-Stokes Equations (NSE) is the cornerstone in the field of Fluid Mechanics and is defined by a set of differential equations that describe the motion of incompressible fluids.…”
Section: Geometry Modeling Of Ocean Surfacementioning
confidence: 99%
“…The normal field of ocean surface can be calculated by making derivative of equation (8). However, this method results in lots of work load.…”
Section: Generate Normal Map Of Ocean Surfacementioning
confidence: 99%
“…[37] G(x, y) is generated in the Fourier plane, by the well-known device of representing the field as a Fourier series [Ben-Yosef et al, 1983;Bell, 1987]. To do so, the Fourier transform C(u, v) of the covariance function c G (x, y) is required.…”
Section: Stochastic Modeling Of Rainy Structures At Large Scalementioning
confidence: 99%